Temporal changes in the debris flow threshold under the effects of ground freezing and sediment storage on Mt. Fuji

<p>Debris flows are one of the most destructive sediment transport processes in mountainous areas because of their large volume, high velocity, and kinematic energy. Debris flow activity varies over time and is affected by changes in hydrogeomorphic processes in the initiation zone. To clarify...

Full description

Bibliographic Details
Main Authors: F. Imaizumi, A. Ikeda, K. Yamamoto, O. Ohsaka
Format: Article
Language:English
Published: Copernicus Publications 2021-11-01
Series:Earth Surface Dynamics
Online Access:https://esurf.copernicus.org/articles/9/1381/2021/esurf-9-1381-2021.pdf